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  • 1
    Publication Date: 2020-09-28
    Description: Reconstructions of global hydroclimate during the Common Era (CE; the past ∼2000 years) are important for providing context for current and future global environmental change. Stable isotope ratios in water are quantitative indicators of hydroclimate on regional to global scales, and these signals are encoded in a wide range of natural geologic archives. Here we present the Iso2k database, a global compilation of previously published datasets from a variety of natural archives that record the stable oxygen (δ18O) or hydrogen (δ2H) isotopic compositions of environmental waters, which reflect hydroclimate changes over the CE. The Iso2k database contains 759 isotope records from the terrestrial and marine realms, including glacier and ground ice (210); speleothems (68); corals, sclerosponges, and mollusks (143); wood (81); lake sediments and other terrestrial sediments (e.g., loess) (158); and marine sediments (99). Individual datasets have temporal resolutions ranging from sub-annual to centennial and include chronological data where available. A fundamental feature of the database is its comprehensive metadata, which will assist both experts and nonexperts in the interpretation of each record and in data synthesis. Key metadata fields have standardized vocabularies to facilitate comparisons across diverse archives and with climate-model-simulated fields. This is the first global-scale collection of water isotope proxy records from multiple types of geological and biological archives. It is suitable for evaluating hydroclimate processes through time and space using large-scale synthesis, model–data intercomparison and (paleo)data assimilation. The Iso2k database is available for download at https://doi.org/10.25921/57j8-vs18 (Konecky and McKay, 2020) and is also accessible via the NOAA/WDS Paleo Data landing page: https://www.ncdc.noaa.gov/paleo/study/29593 (last access: 30 July 2020).
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 2
    Publication Date: 2019-10-24
    Description: A new annually resolved sedimentary record of Southern Hemisphere mid-latitude hydroclimate was recovered from Lake Ohau, South Island, New Zealand, in March 2016. The Lake Ohau Climate History (LOCH) project acquired cores from two sites (LOCH-1 and -2) that preserve sequences of laminated mud that accumulated since the lake formed similar to 17 000 years ago. Cores were recovered using a purpose-built barge and drilling system designed to recover soft sediment from thick sedimentary sequences in lake systems up to 150m deep. This system can be transported in two to three 40 ft long shipping containers and is suitable for use in a range of geographic locations. A comprehensive suite of data has been collected from the sedimentary sequence using state-of-the-art analytical equipment and techniques. These new observations of past environmental variability augment the historical instrumental record and are currently being integrated with regional climate and hydrological modelling studies to explore causes of variability in extreme/flood events over the past several millennia.
    Description: Published
    Description: 41-50
    Description: 4A. Oceanografia e clima
    Description: 5A. Paleoclima e ricerche polari
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2019-07-17
    Description: Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and 1880, punctuated in some regions by warm decades during the eighteenth century. The transition to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or the Southern Hemisphere regions. Recent warming reversed the long-term cooling; during the period ad 1971–2000, the area-weighted average reconstructed temperature was higher than any other time in nearly 1,400 years.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 4
    Publication Date: 2017-07-21
    Description: Reproducible climate reconstructions of the Common Era (1 CE to present) are key to placing industrial-era warming into the context of natural climatic variability. Here we present a community-sourced database of temperature-sensitive proxy records from the PAGES2k initiative. The database gathers 692 records from 648 locations, including all continental regions and major ocean basins. The records are from trees, ice, sediment, corals, speleothems, documentary evidence, and other archives. They range in length from 50 to 2000 years, with a median of 547 years, while temporal resolution ranges from biweekly to centennial. Nearly half of the proxy time series are significantly correlated with HadCRUT4.2 surface temperature over the period 1850–2014. Global temperature composites show a remarkable degree of coherence between high- and low-resolution archives, with broadly similar patterns across archive types, terrestrial versus marine locations, and screening criteria. The database is suited to investigations of global and regional temperature variability over the Common Era, and is shared in the Linked Paleo Data (LiPD) format, including serializations in Matlab, R and Python.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 5
    Publication Date: 2020-06-14
    Description: A comprehensive database of paleoclimate records is needed to place recent warming into the longer-term context of natural climate variability. We present a global compilation of quality-controlled, published, temperature-sensitive proxy records extending back 12,000 years through the Holocene. Data were compiled from 679 sites where time series cover at least 4000 years, are resolved at sub-millennial scale (median spacing of 400 years or finer) and have at least one age control point every 3000 years, with cut-off values slackened in data-sparse regions. The data derive from lake sediment (51%), marine sediment (31%), peat (11%), glacier ice (3%), and other natural archives. The database contains 1319 records, including 157 from the Southern Hemisphere. The multi-proxy database comprises paleotemperature time series based on ecological assemblages, as well as biophysical and geochemical indicators that reflect mean annual or seasonal temperatures, as encoded in the database. This database can be used to reconstruct the spatiotemporal evolution of Holocene temperature at global to regional scales, and is publicly available in Linked Paleo Data (LiPD) format.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 6
    Publication Date: 2021-08-25
    Description: The mid-Holocene (6000 years ago) is a standard time period for the evaluation of the simulated response of global climate models using palaeoclimate reconstructions. The latest mid-Holocene simulations are a palaeoclimate entry card for the Palaeoclimate Model Intercomparison Project (PMIP4) component of the current phase of the Coupled Model Intercomparison Project (CMIP6) – hereafter referred to as PMIP4-CMIP6. Here we provide an initial analysis and evaluation of the results of the experiment for the mid-Holocene. We show that state-of-the-art models produce climate changes that are broadly consistent with theory and observations, including increased summer warming of the Northern Hemisphere and associated shifts in tropical rainfall. Many features of the PMIP4-CMIP6 simulations were present in the previous generation (PMIP3-CMIP5) of simulations. The PMIP4-CMIP6 ensemble for the mid-Holocene has a global mean temperature change of −0.3 K, which is −0.2 K cooler than the PMIP3-CMIP5 simulations predominantly as a result of the prescription of realistic greenhouse gas concentrations in PMIP4-CMIP6. Biases in the magnitude and the sign of regional responses identified in PMIP3-CMIP5, such as the amplification of the northern African monsoon, precipitation changes over Europe, and simulated aridity in mid-Eurasia, are still present in the PMIP4-CMIP6 simulations. Despite these issues, PMIP4-CMIP6 and the mid-Holocene provide an opportunity both for quantitative evaluation and derivation of emergent constraints on the hydrological cycle, feedback strength, and potentially climate sensitivity.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 7
    Publication Date: 2022-05-26
    Description: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Scientific Reports 6 (2016): 29587, doi:10.1038/srep29587.
    Description: Interactions between climate, fire and CO2 are believed to play a crucial role in controlling the distributions of tropical woodlands and savannas, but our understanding of these processes is limited by the paucity of data from undisturbed tropical ecosystems. Here we use a 28,000-year integrated record of vegetation, climate and fire from West Africa to examine the role of these interactions on tropical ecosystem stability. We find that increased aridity between 28–15 kyr B.P. led to the widespread expansion of tropical grasslands, but that frequent fires and low CO2 played a crucial role in stabilizing these ecosystems, even as humidity changed. This resulted in an unstable ecosystem state, which transitioned abruptly from grassland to woodlands as gradual changes in CO2 and fire shifted the balance in favor of woody plants. Since then, high atmospheric CO2 has stabilized tropical forests by promoting woody plant growth, despite increased aridity. Our results indicate that the interactions between climate, CO2 and fire can make tropical ecosystems more resilient to change, but that these systems are dynamically unstable and potentially susceptible to abrupt shifts between woodland and grassland dominated states in the future.
    Description: This work was supported by NSF grants EAR0601998, EAR0602355, AGS0402010, ATM0401908, ATM0214525, ATM0096232 and AGS1243125 and a Chevron Centennial Fellowship at the University of Texas at Austin awarded to T.M.S.
    Keywords: Climate-change ecology ; Palaeoclimate
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 8
    Publication Date: 2024-03-02
    Keywords: 06MT15_2; 108-658A; 161-976; 177-1089; 177-1094; A150/180; A180-73; Agulhas Basin; Agulhas Ridge; Alboran Sea; Amazon Fan; AMK-4438; AMK-4442; ANT-IX/4; ANT-VIII/3; ANT-X/5; ANT-XI/2; ANT-XI/4; ANT-XVIII/5a; APSARA2; Atlantic Ridge; Brazil Basin; CALYPSO; Calypso Corer; Canarias Sea; CH69-K09; COMPCORE; Composite Core; Cosmonauts Sea; D117; DRILL; Drilling/drill rig; E45-29; E49-18; East Atlantic; Eastern Rio Grande Rise; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Event label; EW9302; EW9302-JPC8; GC; GeoB1309-2; GeoB1312-2; GeoB1523-1; GeoB2204-2; GIK12392-1; GIK15637-1; GIK17954-2; GIK23414-5; GL-77; global reconstruction; Gravity corer; Gravity corer (Kiel type); IMAGES I; IMAGES III - IPHIS; IMAGES XI - P.I.C.A.S.S.O.; Indian Ocean; Joides Resolution; JPC; Jumbo Piston Core; K708-001; K708-007; KAL; Kasten corer; KL; KOL; Last Interglacial; LATITUDE; Leg108; Leg161; Leg177; LONGITUDE; M12392-1; M15/2; M16/2; M17/2; M23/3; M23414; M25; M35/1; M35027-1; M53; Marion Dufresne (1972); Marion Dufresne (1995); Maurice Ewing; MD00; MD032664; MD03-2664; MD101; MD106; MD132; MD38; MD73025-2; MD84-527; MD84-551; MD952040; MD95-2040; MD972142; MD97-2142; Meteor (1964); Meteor (1986); Meteor Rise; Method comment; MONITOR MONSUN; Newfoundland margin; Northeast Atlantic; Norwegian Sea; Number of points; OSIRIS I; P-013; PC; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); Polarstern; Porto Seamount; PS16; PS16/271; PS16/278; PS16/311; PS16/345; PS1752-1; PS1754-1; PS1768-8; PS1778-5; PS18; PS18/232; PS18/238; PS18/260; PS2076-3; PS2082-1; PS2102-2; PS22/769; PS22/803; PS22 06AQANTX_5; PS2276-4; PS2305-6; PS2489-2; PS2603-3; PS28; PS28/256; PS30; PS30/140; PS58; PS58/271-1; RC08; RC08-145; RC08-39; RC10; RC10-65; RC11; RC1112; RC11-120; RC11-210; RC11-230; RC11-86; RC12; RC12-294; RC12-339; RC13; RC13-205; RC13-228; RC13-229; RC14; RC14-99; RC15; RC15-61; RC17; RC17-69; RC17-98; RC24; RC24-16; Reference/source; Robert Conrad; Sea surface temperature, December-February; Sea surface temperature, December-February, standard deviation; Sea Surface Temperatures; Shona Ridge; Site; SL; SO95; Sonne; South Atlantic Ocean; South China Sea; Southeast Pacific; South Indian Ocean; SST; Super-interglacial; TR126-23; TR126-29; V12; V12-122; V18; V18-68; V19; V19-29; V19-53; V20; V20-120; V21; V21-146; V22; V22-108; V22-174; V22-182; V22-196; V22-38; V23; V23-82; V25; V25-21; V25-56; V25-59; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-127; V28-14; V28-238; V28-304; V28-345; V28-56; V29; V29-179; V29-29; V30; V30-40; V30-49; V32; V32-126; V32-128; V34; V34-88; Vema; Y71-06; Y71-06-12; Y7211; Y7211-1; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 1188 data points
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  • 9
    Publication Date: 2024-02-29
    Keywords: 06MT15_2; 108-658A; 161-975; 161-976; 162-980; A150/180; A180-73; Agulhas Basin; Alboran Sea; Amazon Fan; AMK-4438; AMK-4442; ANT-IX/4; ANT-VIII/3; Atlantic Ocean; Brazil Basin; CALYPSO; Calypso Corer; Canarias Sea; CH69-K09; Charles Darwin; COMPCORE; Composite Core; D117; DRILL; Drilling/drill rig; E45-29; E49-18; East Atlantic; Eastern Rio Grande Rise; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Event label; EW9302; EW9302-JPC8; GC; GeoB1309-2; GeoB1312-2; GeoB1523-1; GeoB2204-2; GIK12392-1; GIK15637-1; GIK17954-2; GIK23323-1; GIK23414-5; GL-77; global reconstruction; Gravity corer; Gravity corer (Kiel type); IMAGES I; IMAGES II; IMAGES III - IPHIS; IMAGES XI - P.I.C.A.S.S.O.; Indian Ocean; Joides Resolution; JPC; JPC37; Jumbo Piston Core; K708-001; K708-007; KAL; KAL15; Kasten corer; Kasten corer 15 cm; KL; KOL; Last Interglacial; LATITUDE; Leg108; Leg161; Leg162; Le Suroît; LONGITUDE; M12392-1; M15/2; M16/2; M17/2; M23/3; M23414; M25; M35/1; M35027-1; M53; M7/4; Marion Dufresne (1972); Marion Dufresne (1995); Maurice Ewing; MD00; MD032664; MD03-2664; MD101; MD105; MD106; MD132; MD73025-2; MD952040; MD95-2040; MD962085; MD96-2085; MD972142; MD97-2142; Meteor (1964); Meteor (1986); Meteor Rise; Method comment; MONITOR MONSUN; NA87-25; NEAP; NEAP-18K; Newfoundland margin; North Atlantic; Northeast Atlantic; Norwegian Sea; Number of points; off Orange River; OSIRIS I; P-013; PALEOCINAT; PC; Piston corer; Piston corer (BGR type); Piston corer (Kiel type); Polarstern; Porto Seamount; PS16; PS16/278; PS1754-1; PS18; PS18/232; PS2076-3; RC08; RC08-145; RC08-39; RC10; RC10-65; RC11; RC1112; RC11-120; RC11-210; RC11-230; RC11-86; RC12; RC12-294; RC12-339; RC13; RC13-205; RC13-228; RC13-229; RC14; RC14-99; RC15; RC15-61; RC17; RC17-69; RC17-98; RC24; RC24-16; Reference/source; Robert Conrad; Sea surface temperature, June-August; Sea surface temperature, June-August, standard deviation; Sea Surface Temperatures; Site; SL; SO95; Sonne; South Atlantic Ocean; South China Sea; SST; SU90-03; Super-interglacial; TR126-23; TR126-29; V12; V12-122; V18; V18-68; V19; V19-29; V19-53; V20; V20-120; V21; V21-146; V22; V22-108; V22-174; V22-182; V22-196; V22-38; V23; V23-82; V25; V25-21; V25-56; V25-59; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-127; V28-14; V28-238; V28-304; V28-345; V28-56; V29; V29-179; V29-29; V30; V30-40; V30-49; V32; V32-126; V32-128; V34; V34-88; Vema; Western Basin; Y71-06; Y71-06-12; Y7211; Y7211-1; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 1104 data points
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  • 10
    Publication Date: 2024-02-29
    Keywords: 145-882; 167-1019C; 167-1020; 177-1090; 177-1094; 181-1123; 90-593_Site; Agulhas Basin; Agulhas Ridge; AMK-4438; AMK-4442; ANT-IX/4; ANT-VIII/3; ANT-XI/2; ANT-XXVI/2; APSARA4; C9001C; CALYPSO; CALYPSO2; Calypso Corer; Calypso Corer II; CH69-K09; Chatham Rise; COMPCORE; Composite Core; Core; CORE; D117; DRILL; Drilling/drill rig; E45-29; E49-18; Eirik Drift; ELT49; ELT49.017-PC; Eltanin; Event label; EW9302; EW9302-JPC8; FR1/94-GC3; GC; GIK23414-5; global reconstruction; Glomar Challenger; Gravity corer; Gravity corer (Kiel type); IMAGES I; IMAGES III - IPHIS; IMAGES XI - P.I.C.A.S.S.O.; Indian Ocean; Joides Resolution; JPC; Jumbo Piston Core; K708-001; K708-007; KALMAR II; KL; Last Interglacial; LATITUDE; Leg145; Leg167; Leg177; Leg181; Leg90; LONGITUDE; M17/2; M23414; Marion Dufresne (1972); Marion Dufresne (1995); MATACORE; Maurice Ewing; MD00; MD032664; MD03-2664; MD062986; MD06-2986; MD101; MD106; MD132; MD152; MD73025-2; MD88-770; MD952040; MD95-2040; MD972106; MD97-2106; MD972108; MD97-2108; MD972120; MD97-2120; Meteor (1986); Meteor Rise; Method comment; MUC; MultiCorer; Newfoundland margin; North Pacific Ocean; Northwestern Pacific Ocean; Norwegian Sea; Number of points; OSIRIS I; P-013; PC; Piston corer; Piston corer (BGR type); Polarstern; Porto Seamount; PS16; PS16/278; PS1754-1; PS18; PS18/232; PS2076-1; PS2489-2; PS28; PS28/256; PS75/034-2; PS75 BIPOMAC; RC08; RC08-39; RC11; RC1112; RC11-120; RC15; RC15-61; Reference/source; Robert Conrad; Sea surface temperature, annual mean; Sea Surface Temperatures; Shirshov Ridge; Site; SL; SO136; SO136_003GC; SO201/2; SO201-2-85; Sonne; South Atlantic Ocean; South Pacific; South Pacific/Tasman Sea/PLATEAU; South Pacific Ocean; South Tasman Rise; Southwest Pacific Ocean; SST; SU90/08; Super-interglacial; Tasman Sea; TASQWA; Temperature, difference; TSP-2PC; V18; V18-68; V20; V20-120; V22; V22-108; V23; V23-82; V27; V27-116; V27-20; V27-60; V27-86; V28; V28-14; V28-56; V29; V29-179; V30; V30-97; Vema; Y7211; Y7211-1; Y9; Y9_core; Yaquina
    Type: Dataset
    Format: text/tab-separated-values, 378 data points
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